Judith Riyer Beds
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Word Definitions
PAGE 1 OF 12 WORD DEFINITIONS The Catholic Words Memory Match Card Game, a fun way for the entire family—or classroom— to learn new Catholic vocabulary words! Instilling a love and reverence for the faith should begin at an early age. This game was borne out of my own desire to do just that for my own children. The Catholic Words Memory Match Card Game will provide parents, grandparents, teachers, homeschoolers, Dan Gonzalez, his wife Elisa and their catechists and youth ministers a fun way to help teach Catholic vocabulary words. two children Matthew and Zoe. A FUN WAY TO LEARN Watch your little one’s excitement at Mass when they recognize the vessels, objects and vestments With these free printable definitions, the game used in the liturgy. Introducing these words will cards become flash cards. help prepare them to receive the Sacraments and Show a card and read its definition. Let the inaugurate a lifelong journey of learning about the child see the picture of the real-world object. wonders of their Catholic faith. Discuss where the object is seen at your local May God bless you and those entrusted to your care. parish or in the home. Take the cards with you to church and point out the items before or after Mass. Then, let the games begin! Catholic Words Memory Match is an addictive way to learn new Catholic vocabulary words! Dan Gonzalez Advent Wreath: A wreath usually made Alb: A white robe with long sleeves worn by the Altar Bells: A bell or set of bells rung of holly or evergreen branches that hold three priest under his chasuble and the deacon under immediately after the consecration of each purple candles and a rose one. -
Six Adventure Road Trips
Easy Drives, Big Fun, and Planning Tips Six Adventure Road Trips DAY HIKES, FLY-FISHING, SKIING, HISTORIC SITES, AND MUCH MORE A custom guidebook in partnership with Montana Offi ce of Tourism and Business Development and Outside Magazine Montana Contents is the perfect place for road tripping. There are 3 Glacier Country miles and miles of open roads. The landscape is stunning and varied. And its towns are welcoming 6 Roaming the National Forests and alluring, with imaginative hotels, restaurants, and breweries operated by friendly locals. 8 Montana’s Mountain Yellowstone and Glacier National Parks are Biking Paradise the crown jewels, but the Big Sky state is filled with hundreds of equally awesome playgrounds 10 in which to mountain bike, trail run, hike, raft, Gateways to Yellowstone fish, horseback ride, and learn about the region’s rich history, dating back to the days of the 14 The Beauty of Little dinosaurs. And that’s just in summer. Come Bighorn Country winter, the state turns into a wonderland. The skiing and snowboarding are world-class, and the 16 Exploring Missouri state offers up everything from snowshoeing River Country and cross-country skiing to snowmobiling and hot springs. Among Montana’s star attractions 18 Montana on Tap are ten national forests, hundreds of streams, tons of state parks, and historic monuments like 20 Adventure Base Camps Little Bighorn Battlefield and the Lewis and Clark National Historic Trail. Whether it’s a family- 22 friendly hike or a peaceful river trip, there’s an Montana in Winter experience that will recharge your spirit around every corner in Montana. -
Stratigraphy, Age and Correlation of the Upper Cretaceous Tohatchi Formation, Western New Mexico Spencer G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/54 Stratigraphy, age and correlation of the Upper Cretaceous Tohatchi Formation, western New Mexico Spencer G. Lucas, Dennis R. Braman, and Justin A. Spielmann, 2003, pp. 359-368 in: Geology of the Zuni Plateau, Lucas, Spencer G.; Semken, Steven C.; Berglof, William; Ulmer-Scholle, Dana; [eds.], New Mexico Geological Society 54th Annual Fall Field Conference Guidebook, 425 p. This is one of many related papers that were included in the 2003 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. -
APS Bulletin 28(1) March 2013
Palæontological Society Bulletin AlbertaVOLUME 28 • NUMBER 1 www.albertapaleo.org MARCH 2013 ALBERTA PALÆONTOLOGICAL SOCIETY OFFICERS MEMBERSHIP: Any person with a sincere interest in President Wayne Braunberger (403) 278-5154 palaeontology is eligible to present their application for Vice-President Cory Gross (403) 617-2079 membership in the Society. (Please enclose membership Treasurer Mona Marsovsky (403) 547-0182 dues with your request for application.) Secretary Arnold Ingelson (403) 249-6748 Past-President Dan Quinsey (403) 247-3022 Single membership $20.00 annually Family or Institution $25.00 annually DIRECTORS Editor Howard Allen (403) 274-1858 THE BULLETIN WILL BE PUBLISHED QUARTERLY: Membership Vaclav Marsovsky (403) 547-0182 March, June, September and December. Deadline for sub- Programs Harold Whittaker (403) 286-0349 mitting material for publication is the 15th of the month Field Trips (To volunteer contact the President) prior to publication. COMMITTEES Society Mailing Address: Fossil Collection Howard Allen (403) 274-1858 Alberta Palaeontological Society Library Reg Spratley (403) 263-0556 P.O. Box 35111, Sarcee Postal Outlet Public Outreach Cory Gross (403) 617-2079 Calgary, Alberta, Canada T3E 7C7 Social Dan Quinsey (403) 247-3022 (Web: www.albertapaleo.org) Symposium Vaclav Marsovsky (403) 547-0182 Website Vaclav Marsovsky (403) 547-0182 Material for the Bulletin: The Society was incorporated in 1986, as a non-profit Howard Allen, Editor, APS organization formed to: 7828 Hunterslea Crescent, N.W. Calgary, Alberta, Canada T2K 4M2 a. Promote the science of palaeontology through study (E-mail: [email protected]) and education. b. Make contributions to the science by: NOTICE: Readers are advised that opinions expressed in 1) Discovery 2) Collection 3) Description the articles are those of the author and do not necessarily 4) Education of the general public reflect the viewpoint of the Society. -
Theropod Teeth from the Upper Maastrichtian Hell Creek Formation “Sue” Quarry: New Morphotypes and Faunal Comparisons
Theropod teeth from the upper Maastrichtian Hell Creek Formation “Sue” Quarry: New morphotypes and faunal comparisons TERRY A. GATES, LINDSAY E. ZANNO, and PETER J. MAKOVICKY Gates, T.A., Zanno, L.E., and Makovicky, P.J. 2015. Theropod teeth from the upper Maastrichtian Hell Creek Formation “Sue” Quarry: New morphotypes and faunal comparisons. Acta Palaeontologica Polonica 60 (1): 131–139. Isolated teeth from vertebrate microfossil localities often provide unique information on the biodiversity of ancient ecosystems that might otherwise remain unrecognized. Microfossil sampling is a particularly valuable tool for doc- umenting taxa that are poorly represented in macrofossil surveys due to small body size, fragile skeletal structure, or relatively low ecosystem abundance. Because biodiversity patterns in the late Maastrichtian of North American are the primary data for a broad array of studies regarding non-avian dinosaur extinction in the terminal Cretaceous, intensive sampling on multiple scales is critical to understanding the nature of this event. We address theropod biodiversity in the Maastrichtian by examining teeth collected from the Hell Creek Formation locality that yielded FMNH PR 2081 (the Tyrannosaurus rex specimen “Sue”). Eight morphotypes (three previously undocumented) are identified in the sample, representing Tyrannosauridae, Dromaeosauridae, Troodontidae, and Avialae. Noticeably absent are teeth attributed to the morphotypes Richardoestesia and Paronychodon. Morphometric comparison to dromaeosaurid teeth from multiple Hell Creek and Lance formations microsites reveals two unique dromaeosaurid morphotypes bearing finer distal denticles than present on teeth of similar size, and also differences in crown shape in at least one of these. These findings suggest more dromaeosaurid taxa, and a higher Maastrichtian biodiversity, than previously appreciated. -
The Transition from the Judith River Formation to the Bearpaw Shale
The transition from the Judith River Formation to the Bearpaw Shale (Campanian), north-central Montana by Roger Elmer Braun A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Roger Elmer Braun (1983) Abstract: The upper 15 m of the Judith River Formation on and adjacent to the Fort Belknap Indian Reservation, north-central Montana is composed mostly of overbank mudrock, siltstone, fine-grained sandstone, and coal, with some cross-stratified channel sandstone in the lower part. The lower 15 m of the overlying Bearpaw Shale is a transgressive deposit composed primarily of concretionary silty shale with some clayey, silty sandstone zones and one bentonite bed. The source area for both formations was primarily in western Montana and Idaho, with the Elkhorn Mountains volcanics a major source of debris. The contact between the Judith River and Bearpaw formations is abrupt and lacks a transgressive sandstone facies. The transgression of the Bearpaw sea across the study area is considered to have been a nearly isochronous event because of the nature of the transition, small east-west differences in thickness between marker horizons, and similar elevations of the contact from east to west across undeformed parts of the study area. The Bearpaw transgression was caused mainly by tectonic thickening in the western Cordillera, which created subsidence primarily in the western and central portions of the Western Interior basin. The transgression was a nearly isochronous event that took place approximately 72 m.y. ago according to radiometric age dates on bentonite beds. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
KENNETH CARPENTER, Ph.D. Director and Curator Of
KENNETH CARPENTER, Ph.D. Director and Curator of Paleontology Prehistoric Museum Utah State University - College of Eastern Utah 155 East Main Street Price, Utah 84501 Education May, 1996. Ph.D., Geology University of Colorado, Boulder, CO. Dissertation “Sharon Springs Member, Pierre Shale (Lower Campanian) depositional environment and origin of it' s Vertebrate fauna, with a review of North American plesiosaurs” 251 p. May, 1980. B.S. in Geology, University of Colorado, Boulder, CO. Aug-Dec. 1977 Apprenticeship, Smithsonian Inst., Washington DC Professional Museum Experience 1975 – 1980: University of Colorado Museum, Boulder, CO. 1983 – 1984: Mississippi Museum of Natural History, Jackson, MS. 1984 – 1986: Academy of Natural Sciences of Philadelphia, Philadelphia. 1986: Carnegie Museum of Natural History, Pittsburgh, PA. 1986: Oklahoma Museum of Natural History, Norman, OK. 1987 – 1989: Museum of the Rockies, Bozeman, MT. 1989 – 1996: Chief Preparator, Denver Museum of Nature and Science, Denver, CO. 1996 – 2010: Chief Preparator, and Curator of Vertebrate Paleontology, Denver Museum of Nature and Science, Denver, CO. 2006 – 2007; 2008-2009: Acting Department Head, Chief Preparator, and Curator of Vertebrate Paleontology, Denver Museum of Nature and Science, Denver, CO. 2010 – present: Director, Prehistoric Museum, Price, UT 2010 – present: Associate Vice Chancellor, Utah State University Professional Services: 1991 – 1998: Science Advisor, Garden Park Paleontological Society 1994: Senior Organizer, Symposium "The Upper Jurassic Morrison Formation: An Interdisciplinary Study" 1996: Scientific Consultant Walking With Dinosaurs , BBC, England 2000: Scientific Consultant Ballad of Big Al , BBC, England 2000 – 2003: Associate Editor, Journal of Vertebrate Paleontology 2001 – 2003: Associate Editor, Earth Sciences History journal 2003 – present: Scientific Advisor, HAN Project 21 Dinosaur Expos, Tokyo, Japan. -
North-Central Montana
Petrology of the Eagle Sandstone, Bearpaw Mountains Area, North-Central Montana By DONALD L. GAUTIER INVESTIGATIONS OF SHALLOW GAS RESERVOIRS IN THE NORTHERN GREAT PLAINS GEOLOGICAL SURVEY BULLETIN 1521 Prepared in cooperation with the U. S. Depart1Tl£nt of Energy Composition and burial history of an important conventional shallow methane reservoir in the northern Great Plains UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data . Gautier, Donald L. Petrology of the Eagle Sandstone, Bearpaw Mountains area, north-central Montana. (Investigations of shallow gas reservoirs in the northern Great Plains) (Geological Survey Bulletin 1521) Bibliography: p. 52 1. Sandstone-Montana-Bearpaw Mountains region. 2. Gas, Natural-Geology Montana-Bearpaw Mountains region. I. Title. II. Series. III. Series: Geological Survey Bulletin 1521. QE75.B9 no. 1521 [QE471.15.S25] 557.3s 81-607963 [552'.5] AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Absuact:---------------------------------------------------- 1 In~uction------------------------------------------------- 2 ~~un~--------------------------------------------- 4 Acknowledgments-------------------------------------- 5 Geologic Setting----------------------------------- 6 Hydrocarbons in the Eagle Sandstone------------------------ 8 Lithology---------------------------------------- -
Pope Addresses Vatican Reforms Aimed at Curbing Corruption, Abuse
Pope addresses Vatican reforms aimed at curbing corruption, abuse VATICAN CITY (CNS) — While financial reforms in the Vatican are progressing steadily, cases involving corruption and malfeasance in the Eternal City are “a disease that we relapse into,” Pope Francis said. In a wide-ranging interview broadcast Sept. 1 by COPE, the Spanish radio station owned by the Spanish bishops’ conference, Pope Francis said changes made in the Vatican’s financial laws have allowed prosecutors to “become more independent” in their investigations. “Let’s hope that these steps we are taking … will help to make these events happen less and less,” he said. During the interview, the pope was asked about the Vatican trial against 10 individuals and entities, including Cardinal Angelo Becciu, former prefect of the Congregation for Saints’ Causes, on charges ranging from embezzlement to money laundering and abuse of office. The charges stemmed from a Vatican investigation into how the Secretariat of State used $200 million to finance a property development project in London’s posh Chelsea district and incurred millions of dollars in debt. At the time, then- Archbishop Becciu served as “sostituto,” the No. 3 position in the Vatican Secretariat of State. Cardinal Becciu was forced to offer his resignation to the pope in September 2020, after he was accused of embezzling an estimated 100,000 euros of Vatican funds and redirecting them to Spes, a Caritas organization run by his brother, Tonino Becciu, in his home Diocese of Ozieri, Sardinia. The pope told COPE he authorized the Vatican’s investigation into the property deal as a sign that he was “not afraid of transparency or the truth.” “Sometimes it hurts a lot, but the truth is what sets us free,” he said. -
Church and Liturgical Objects and Terms
Church and Liturgical Objects and Terms Liturgical Objects Used in Church The chalice: The The paten: The vessel which golden “plate” that holds the wine holds the bread that that becomes the becomes the Sacred Precious Blood of Body of Christ. Christ. The ciborium: A The pyx: golden vessel A small, closing with a lid that is golden vessel that is used for the used to bring the distribution and Blessed Sacrament to reservation of those who cannot Hosts. come to the church. The purificator is The cruets hold the a small wine and the water rectangular cloth that are used at used for wiping Mass. the chalice. The lavabo towel, The lavabo and which the priest pitcher: used for dries his hands after washing the washing them during priest's hands. the Mass. The corporal is a square cloth placed The altar cloth: A on the altar beneath rectangular white the chalice and cloth that covers paten. It is folded so the altar for the as to catch any celebration of particles of the Host Mass. that may accidentally fall The altar A new Paschal candles: Mass candle is prepared must be and blessed every celebrated with year at the Easter natural candles Vigil. This light stands (more than 51% near the altar during bees wax), which the Easter Season signify the and near the presence of baptismal font Christ, our light. during the rest of the year. It may also stand near the casket during the funeral rites. The sanctuary lamp: Bells, rung during A candle, often red, the calling down that burns near the of the Holy Spirit tabernacle when the to consecrate the Blessed Sacrament is bread and wine present there. -
The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M
The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M. Gilbert Department of Geological Sciences, University of Saskatchewan; [email protected] Summary The Upper Cretaceous Dinosaur Park Formation (DPF) is a south- and eastward-thinning fluvial to marginal marine clastic-wedge in the Western Canadian Sedimentary Basin. The DPF is overlain by the Bearpaw Formation (BF), a fully marine clastic succession representing the final major transgression of the epicontinental Western Interior Seaway (WIS) across western North America. In southwestern Saskatchewan, the DPF is comprised of marginal marine coal, carbonaceous shale, and heterolithic siltstone and sandstone grading vertically into marine sandstone and shale of the Bearpaw Formation. Due to Saskatchewan’s proximity to the paleocoastline, 5th order transgressive cycles resulted in the deposition of multiple coal seams (Lethbridge Coal Zone; LCZ) in the upper two-thirds of the DPF in the study area. The estimated total volume of coal is 48109 m3, with a gas potential of 46109 m3 (Frank, 2005). The focus of this study is to characterize the facies and facies associations of the DPF, the newly erected Manâtakâw Member, and the lower BF in the Cypress Hills region of southwestern Saskatchewan utilizing core, outcrop, and geophysical well log data. This study provides a comprehensive sequence stratigraphic overview of the DPF-BF transition in Saskatchewan and the potential for coalbed methane exploration. Introduction The Dinosaur Park and Bearpaw Formations in Alberta, and its equivalents in Montana, have been the focus of several sedimentologic and stratigraphic studies due to exceptional outcrop exposure and extensive subsurface data (e.g., McLean, 1971; Wood, 1985, 1989; Eberth and Hamblin, 1993; Tsujita, 1995; Catuneanu et al., 1997; Hamblin, 1997; Rogers et al., 2016).